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@ARTICLE{Brasseur:54142,
      author       = {Brasseur, G. P. and Schultz, M. and Granier, C. and
                      Saunois, M. and Botzet, T. M. and Roeckner, E. and Walters,
                      S.},
      title        = {{I}mpact of {C}limate {C}hange on the {F}uture {C}hemical
                      {C}ompositions of the {G}lobal {T}roposphere},
      journal      = {Journal of climate},
      volume       = {19},
      issn         = {0894-8755},
      address      = {Boston, Mass. [u.a.]},
      publisher    = {AMS},
      reportid     = {PreJuSER-54142},
      pages        = {3932 - 3951},
      year         = {2006},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {A global chemical transport model of the atmosphere [the
                      Model for Ozone and Related Tracers, version 2 (MOZART-2)]
                      driven by prescribed surface emissions and by meteorological
                      fields provided by the ECHAM5/Max Planck Institute Ocean
                      Model (MPI-OM-1) coupled atmosphere-ocean model is used to
                      assess how expected climate changes (2100 versus 2000
                      periods) should affect the chemical composition of the
                      troposphere. Calculations suggest that ozone changes
                      resulting from climate change only are negative in a large
                      fraction of the troposphere because of enhanced
                      photochemical destruction by water vapor. In the Tropics,
                      increased lightning activity should lead to larger ozone
                      concentrations. The magnitude of the climate-induced ozone
                      changes in the troposphere remains smaller than the changes
                      produced by enhanced anthropogenic emissions when the
                      Special Report on Emission Scenarios (SRES) A2P is adopted
                      to describe the future evolution of these emissions.
                      Predictions depend strongly on future trends in atmospheric
                      methane levels, which are not well established. Changes in
                      the emissions of NOx by bacteria in soils and of nonmethane
                      hydrocarbons by vegetation associated with climate change
                      could have a significant impact on future ozone levels.},
      keywords     = {J (WoSType)},
      cin          = {ICG-II},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB48},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK406},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000240228000010},
      doi          = {10.1175/JCLI3832.1},
      url          = {https://juser.fz-juelich.de/record/54142},
}